平流的的英文

• advectional
• advective

• "平流"英文翻译    advection
• "的"英文翻译    4次方是 The fourth power of 2 i ...
• "平流" 英文翻译 :    [海洋学] advection
• "层流；平流" 英文翻译 :    laminar flow
• "冷平流" 英文翻译 :    cold advection
• "滤波，平流" 英文翻译 :    smoothing
• "暖平流" 英文翻译 :    warm advection
• "平流槽" 英文翻译 :    horizontal flow tank
• "平流层" 英文翻译 :    stratosphere
• "平流区" 英文翻译 :    advection region; advective region
• "平流霜" 英文翻译 :    advective frost
• "平流雾" 英文翻译 :    advection fog; advectionfog
• "平流相" 英文翻译 :    smooth phase
• "平流支" 英文翻译 :    stratosphere
• "热平流" 英文翻译 :    thermal advection
• "水平流" 英文翻译 :    horizontal current; horizontal flow
• "回流的, 反流的" 英文翻译 :    regurgitant
• "绕流的，周流的" 英文翻译 :    circumfluent
• "周流的,环流的" 英文翻译 :    circumfluent
• "背流的" 英文翻译 :    lee
• "奔流的" 英文翻译 :    torrential
• "层流的" 英文翻译 :    laminal; laminary
• "常流的" 英文翻译 :    ever flowing
• "单流的" 英文翻译 :    singleflow; uniflow
• "倒流的" 英文翻译 :    refluent

• The in of nonlinear advection into the model weakens the intensity of both inward and outward propagation of vorticity , but makes the inward propagation up to a posi
  非线性平流的引进，使涡量向内区传输以及向外传输的强度均减弱：但内传的涡量更加接近于台风中心。
• The azimuthally linear advection may results in that the meso - scale vortex of initially circular shape becomes the elongated and spiral vorticity bands ; the radial linear advection may transfer the vorticity of the outer region towards the center of the typhoon
  沿e方向的线性平流可使初始圆形的中尺度涡旋演变为狭长的螺旋状的涡量带;沿径向线性平流的引进可使外区涡量向台风中心方向传播。
• The results show that a warm high ridge at the middle level and transformed surface cold high over the plain provide a good background condition ; a cooling process produced by net surface radiation fluxes is the trigger and strengthening mechanism for the fog event ; the subsidence flow at the middle and low tropospheric levels is favorable for the setting - up and maintenance of stable stratification at the boundary layer and weak wind condition at the ground layer over the fog region ; the transportation of weak warm advection at lower levels and weak lift motion at the boundary layer play a very important role to the long maintenance of the fog event ; the intrusion of north wind accompanied by cold advection is a main dynamic factor of the fog dissipation
  结果表明：在中高层暖性高压脊及地面变性冷高压稳定维持的大尺度背景条件下，地表净辐射引起的近地层冷却是大雾过程的触发和加强机制；中低空下沉气流的存在有助于近地层的弱风条件和稳定层结的建立；低层暖平流的输入和边界层的浅层抬升是大雾长时间持续的原因；伴随冷空气南下的偏北大风是驱使大雾消散的动力因子。
• The non - local nonlinear advection possesses the duality : on one hand , compared with the linear circumstance , it increases the inward - propagation of vorticity , thus favorable to the strengthening of the typhoon ; however on the other hand , the inward - propagating vorticity destroys the concentric circle structure of the typhoon circulation , leading to the weakening of the typhoon
  非局域非线性平流的作用具有两重性:一方面，与线性情况相比，可使内传涡量增加，这有利于台风增强;另一方面内传的涡量又破坏了台风环流的同心圆结构，这使台风趋于减弱。
• There are two parts in this paper : firstly , a set of single doppler velocity models are presented for typical ambient windfields that include those of being uniform horizontally , macroscale convergence and divergence , which overlap warm and cold advection . which are marked by different signatures in the single doppler velocity field . the models proposed can help users identify useful information from the dopple velocity patterns
  本论文包括两个部分：第一篇通过对典型风场的单多普勒天气雷达径向速度图象进行模拟，典型风场包括水平均匀一致的风场、非均匀水平风场的大尺度运动的辐合辐散风场以及大尺度运动的辐合辐散风场与冷暖平流的迭加等。
• The above analysis showed that this heavy rainfall event took on obvious meso - scale characters and was the combination of the three flows , so we can deduce : ( 1 ) surface southeasterly wind and topography may play the main role in this event ; ( 2 ) the easterly cold air rushing into the southern shaanxi province in the lower troposphere was strongly relative to the form of surface cold - front type of occlusion ; ( 3 ) there were two reasons for the secondary circulation ' s strengthen in the evening , one was the effect of a mountain - valley wind and the other may be latent heat leading to ascending motion ; ( 4 ) the shape of potential instability stratification corresponded well with the development of the warm - moisture advection ; and ( 5 ) the vapor providing essential thermodynamics was transported by a southwesterly low - level jet from the bay of bengal and the south china sea . furthermore , with the effect of terrain , the southern shaanxi province became the center of this extremely heavy rain process
  中尺度结构分析表明，本次暴雨具有明显的中尺度特征，是由三支气流共同作用的结果，分析发现( 1 )地面东南风和地形在这次大暴雨过程起主要作用； ( 2 )东路冷空气主要是通过中低层侵入陕南地区的，并与地面冷式锢囚锋的形成密不可分； ( 3 )夜博士论文:中尺度地形对陕南暴雨的影响研究间垂直次级环流发展加强可能有两个原因，一个是由于地形山谷风的作用，另一个是降水的潜热释放激发了上升运动: ( 4 )位势不稳定层结的形成与低层暖湿平流的发展有很好的对应关系; ( 5 )本次暴雨的水汽主要靠偏南风急流将孟加拉湾和中国南海的水汽输送至西北地区东部，为暴雨的发生提供了必要热力条件。
• A very much different fluxes model was suggested for remote sensing estimation , which takes account of the effects of advections in vertically or horizontally anisothermal vegetations . the inter - exchange of heat can result in lower total sensible heat flux and higher total latent heat flux of the considered areas . this method is designed technically for the simulations of pixel , is a try of new generation effluxes model
  针对遥感基于像元计算的特点，提出一种全新的通量计算方法，模型的结构和思路专为遥感像元面上计算的特点而设计，主要考虑由地表非均匀和不连续性引起的像元内部热量交换? ?局地微平流对显热和潜热通量的影响，验证表明，这种考虑平流的非均匀模型可以较好地模拟地表非均匀状态下的热量通量。

• 平流的的法语：advectif